Bhutan, country of south-central Asia, located on the eastern ridges of the Himalayas. Historically a remote kingdom, Bhutan became less isolated in the second half of the 20th century, and consequently the pace of change began to accelerate. With improvements in transportation, by the early 21st century a trip from the Indian border to the Bhutanese capital, Thimphu, that once took six days by mule could be made in just a few hours by car along a winding mountain road from the border town of Phuntsholing. The governmental structure also changed radically. Reforms initiated by King Jigme Dorji Wangchuk (reigned 1952–72) in the 1950s and ’60s led to a shift away from absolute monarchy in the 1990s and toward the institution of multiparty parliamentary democracy in 2008.

The economic core of Bhutan lies in the fertile valleys of the Lesser Himalayas, which are separated from one another by a series of high and complex interconnecting ridges extending across the country from north to south. The political nucleus of Bhutan is centred in the Paro and Thimphu valleys in the Lesser Himalayan region. Its location between the Assam-Bengal Plain of India to the south and the Plateau of Tibet of southwestern China to the north gives the country considerable geopolitical significance.

Land

Bhutan’s northern and western boundary with the Tibet Autonomous Region (part of China), although undefined, generally follows the crest of the Great Himalayas. In the Duars Plain to the south of the Himalayan range lies Bhutan’s boundary with the Indian states of West Bengal and Assam. Bhutan borders the Indian states of Arunachal Pradesh to the east and Sikkim to the southwest.

Relief

The northern part of Bhutan lies within the Great Himalayas; the snowcapped peaks in this region reach an elevation of more than 24,000 feet (7,300 metres). High valleys occur at elevations of 12,000 to 18,000 feet (3,700 to 5,500 metres), running down from the great northern glaciers. Alpine pastures on the high ranges are used for grazing yaks in the summer months. To the north of the Great Himalayas are several “marginal” mountains of the Plateau of Tibet that form the principal watershed between the northward- and the southward-flowing rivers. A dry climate is characteristic of the Great Himalayan region.

Until about 1960 the tempo of life in the Great Himalayas continued much as it had for centuries. Long relatively undisturbed in their ways, Bhutanese traders carried cloth, spices, and grains across the mountain passes into Tibet and brought back salt, wool, and sometimes herds of yaks. The absorption of Tibet by China, however, necessarily pushed Bhutan toward ending its isolation; the event brought major changes to the way of living in those high regions, as military precautions were taken to guard against the potential danger of a Chinese incursion from Tibet.

Spurs from the Great Himalayas radiate southward, forming the ranges of the Lesser Himalayas (also called Inner Himalayas). The north-south ranges of the Lesser Himalayas constitute watersheds between the principal rivers of Bhutan. Differences in elevation and the degree of exposure to moist southwest monsoon winds determine the prevailing vegetation, which ranges from dense forest on the rain-swept windward slopes to alpine vegetation at higher elevations. Several fertile valleys of central Bhutan are in the Lesser Himalayas at elevations varying from 5,000 to 9,000 feet (1,500 to 2,700 metres). These valleys, notably the Paro, Punakha, Thimphu, and Ha, are relatively broad and flat, receive moderate rainfall (from 40 to 50 inches [about 1,000 to 1,270 mm] or less a year), and are fairly well populated and cultivated.

The Duars Plain

South of the Lesser Himalayas and the foothills lies the narrow Duars Plain, which forms a strip 8 to 10 miles (12 to 16 km) wide along the southern border of Bhutan. The Himalayan ranges rise sharply and abruptly from this plain, which constitutes a gateway to the strategic mountain passes (known as dwars or dooars) that lead into the fertile valleys of the Lesser Himalayas. Subject to abundant rainfall (200 to 300 inches [5,100 to 7,600 mm] a year), the entire Duars tract is hot and steamy and is covered with dense semitropical forest and undergrowth.

The northern part of the Duars, immediately bordering the mountains, consists of a rugged, irregular, and sloping surface. At the foot of the mountains, small villages are found in forest clearings, but most of the area is thickly covered with vegetation inhabited by an array of large wild animals. The southern part of the Duars, bordering India, is mostly covered with savanna (grassy parkland) and bamboo jungle. In many areas the savannas have been cleared for rice cultivation. The principal trade routes between central Bhutan and India follow the valleys of the main rivers.

Drainage

Bhutan’s mountainous territory is dissected by numerous rivers. The main rivers from west to east are the Torsa (Amo), Wong (Raidak), Sankosh (Mo), and Manas. All the rivers flow southward from the Great Himalayas and join the Brahmaputra River in India.

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